Measurements · Module 9 of 10
Pressure and Flow Measurement
Pressure is measured by balancing it against a column of fluid, and flow is often measured from the pressure drop across a constriction. Both come back to a height or a pressure difference.
Readiness check
This module measures pressure and flow. Tick only what you can do closed-notes.
- Multiply density, gravity, and height.
- Take a square root of a ratio.
- Recall that pressure rises with fluid depth.
- Recall that a constriction speeds up a flow.
- Recall the density of water and mercury.
The core idea
A manometer measures a pressure difference as a fluid column, Δp = ρgh. A flow through a constriction speeds up and its pressure drops, so Bernoulli gives an ideal velocity v = √(2Δp/ρ); a discharge coefficient corrects for real losses, and the flow rate is Q = CdAv.
manometer: Δp = ρghBernoulli velocity: v = √(2Δp/ρ)flow rate: Q = Cd A vPressure and flow are linked, and both reduce to reading a height or a pressure difference. Pressure comes in three flavours: absolute, measured from vacuum; gauge, measured from atmospheric; and differential, the difference between two points. The simplest instrument is the manometer, a U-tube whose fluid column balances the applied pressure difference, giving Δp = ρgh directly, where ρ is the manometer fluid's density and h the height difference; mercury's high density lets a short column read a large pressure. For higher or dynamic pressures, transducers such as the Bourdon tube and the diaphragm convert pressure into a mechanical deflection sensed electrically, often through a strain-gauge bridge. Flow measurement borrows the same pressure idea. An obstruction meter, an orifice plate or a venturi, narrows the pipe; by continuity the fluid accelerates through the throat, and by Bernoulli its pressure falls, so the measured pressure drop gives an ideal velocity v = √(2Δp/ρ). Real flows lose energy, so a discharge coefficient Cd, found by calibration, scales this to the true flow rate Q = CdAv. A Pitot tube uses the same relation to get a local velocity from the dynamic pressure. Pressure, in short, is the currency of flow measurement.
The skills, taught in order
Five skills measure pressure and turn it into flow.
9.1 Pressure concepts
Absolute pressure is measured from vacuum, gauge from atmospheric, and differential between two points. Naming which one you mean avoids the common error of double counting or omitting atmospheric pressure.
9.2 Manometers
A U-tube manometer balances a pressure difference against a fluid column, so Δp = ρgh. The manometer fluid's density sets the sensitivity: water for small pressures, mercury for large ones in a short tube.
9.3 Pressure transducers
Bourdon tubes and diaphragms deflect under pressure, and that deflection is sensed, often by a strain-gauge bridge, giving an electrical output. Transducers handle high and rapidly changing pressures a manometer cannot.
9.4 Obstruction flow meters
An orifice or venturi constricts the flow; continuity speeds it up and Bernoulli drops its pressure, so the pressure difference gives an ideal velocity v = √(2Δp/ρ). The venturi recovers more pressure; the orifice is cheaper.
| Instrument | Measures | Relation |
|---|---|---|
| Manometer | pressure difference | Δp = ρgh |
| Venturi / orifice | flow rate | Q = CdA√(2Δp/ρ) |
| Pitot tube | local velocity | v = √(2Δp/ρ) |
Pressure difference is the common thread: it gives height, flow rate, or velocity depending on the instrument.
9.5 Discharge coefficient and velocity
Real flow loses energy, so the ideal velocity overstates the truth; the discharge coefficient Cd, from calibration, corrects it, giving Q = CdAv. A Pitot tube applies the same √(2Δp/ρ) to the dynamic pressure for a point velocity.
Engineering connection: a venturi in a pipe with a differential-pressure transducer gives a continuous flow reading, the pressure drop converted to velocity and then to volume flow.
Worked example 1: a mercury manometer
A mercury manometer (ρ = 13600 kg/m3) shows a height difference of 0.05 m. Find the pressure difference, with g = 9.81 m/s2.
- ProblemFind the pressure difference for the manometer in Figure 1.
- Given / findρ = 13600 kg/m3, h = 0.05 m, g = 9.81 m/s2. Find Δp.
- AssumptionsStatic fluid; the manometer fluid is mercury.
- ModelΔp = ρgh.
- EquationsΔp = 13600 × 9.81 × 0.05
- SolveΔp = 6670.8 Pa ≈ 6.67 kPa.
- CheckMercury gives about 133.4 kPa per metre, and 0.05 m of it is about 6.67 kPa, matching.
- ConclusionA 5 cm mercury column reads about 6.67 kPa; water would need a column roughly 13.6 times taller for the same pressure.
Worked example 2: velocity from a pressure drop
Water (ρ = 1000 kg/m3) flows through a venturi with a pressure drop of 5000 Pa across the throat. Find the ideal velocity from Bernoulli.
- ProblemFind the ideal velocity for the venturi in Figure 2.
- Given / findρ = 1000 kg/m3, Δp = 5000 Pa. Find v.
- AssumptionsIdeal, incompressible, frictionless flow; discharge coefficient taken as 1 for the ideal value.
- ModelBernoulli across the constriction gives v = √(2Δp/ρ).
- Equationsv = √(2 × 5000 / 1000)= √10
- Solvev = 3.16 m/s.
- Check2 × 5000 / 1000 = 10, and √10 ≈ 3.16 m/s; a real meter would read Cd times this, a little less.
- ConclusionThe ideal throat velocity is about 3.16 m/s; multiplying by the discharge coefficient and throat area gives the true flow rate.
Misconceptions and diagnostics
| Mistake | Symptom | Diagnostic question | Correction |
|---|---|---|---|
| Gauge versus absolute | Atmospheric pressure mishandled | "From vacuum or from atmosphere?" | State which reference the pressure uses. |
| Wrong manometer density | Pressure off by the density ratio | "Which fluid is in the manometer?" | Use the manometer fluid's density in ρgh. |
| Ideal velocity as true | Flow overstated | "Did I apply Cd?" | Multiply by the discharge coefficient for real flow. |
| Forgetting the square root | Velocity wildly too large | "Is v the root of 2Δp/ρ?" | Velocity is the square root, not 2Δp/ρ itself. |
Practice ladder
A water manometer (ρ = 1000 kg/m3) shows a 0.2 m height difference. Find the pressure difference.
Show answer
Δp = 1000 × 9.81 × 0.2 = 1962 Pa ≈ 1.96 kPa.
Water flows through a venturi with a pressure drop of 8000 Pa. Find the ideal velocity.
Show answer
v = √(2 × 8000 / 1000) = √16 = 4 m/s.
A Pitot tube in air (ρ = 1.2 kg/m3) reads a dynamic pressure of 60 Pa. Find the air velocity.
Show answer
v = √(2 × 60 / 1.2) = √100 = 10 m/s.
Choose an instrument to measure (a) the flow rate in a large water main and (b) the local air speed at a point in a duct. Justify each.
What good work looks like
(a) A venturi or orifice with a differential-pressure transducer, giving whole-pipe flow rate through Q = CdAv; (b) a Pitot tube, giving the local velocity at its tip from the dynamic pressure. A good answer distinguishes bulk flow rate from point velocity.
Working with AI, and proving it yourself
Use AI as an examiner, not a solver
Portfolio task
Work a real pressure or flow measurement: convert a manometer height to pressure, or a pressure drop to a velocity and flow rate.
Retrieval and spaced review
Closed notes. Answer out loud, then reveal.
1. Write the manometer relation.
Δp = ρgh.
2. Write the Bernoulli velocity.
v = √(2Δp/ρ).
3. What does the discharge coefficient do?
Corrects the ideal flow for real energy losses.
4. Absolute, gauge, differential?
From vacuum, from atmospheric, and between two points.
5. What does a Pitot tube give?
A local velocity from the dynamic pressure.
Textbook mapping
This module follows Figliola and Beasley, Theory and Design for Mechanical Measurements, 5th edition. Use these references to read further.
| Topic in this module | Where to read more |
|---|---|
| Pressure concepts and manometers | Figliola and Beasley, Sections 9.2 and 9.3 |
| Pressure transducers | Figliola and Beasley, Section 9.4, Pressure Transducers |
| Obstruction flow meters | Figliola and Beasley, Chapter 10, Flow Measurements |
Section numbers refer to Figliola and Beasley, 5th edition. Any edition with the same chapter titles is equivalent for study.